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Behaviour of oscillations in loop structures above active regions

D.Y. Kolobova,1,∗, N.I. Kobanova,1, A.A. Chelpanova,1, A.A. Kochanova,1, S.A. Anfinogentova,1, S.A. Chupina,1, I.I. Myshyakova,1, V.E. Tomina,1

aRussia, 664033, Irkutsk, Lermontov St., 126-a

Abstract In this study we combine the multiwavelength ultraviolet – optical (Solar Dy- namics Observatory, SDO) and radio (Nobeyama Radioheliograph, NoRH) observations to get further insight into space-frequency distribution of oscil- lations at different atmospheric levels of the . We processed the observa- tional data on NOAA 11711 active region and found oscillations propagating from the photospheric level through the transition region upward into the corona. The power maps of low-frequency (1–2 mHz) oscillations reproduce well the fan-like coronal structures visible in the Fe ix 171 A˚ line. High fre- quency oscillations (5–7 mHz) propagate along the vertical magnetic field lines and concentrate inside small-scale elements in the umbra and at the umbra-penumbra boundary. We investigated the dependence of the domi- nant oscillation frequency upon the distance from the barycentre to estimate inclination of magnetic tubes in higher levels of where it cannot be measured directly, and found that this angle is close to 40° above the umbra boundaries in the transition region. Keywords: Sunspots, Oscillations; Faculae, Oscillations; Magnetic topology; Coronal loops

∗ arXiv:1505.02857v1 [astro-ph.SR] 12 May 2015 Corresponding author Email address: [email protected] (D.Y. Kolobov) 1Institute of Solar-Terrestrial Physics, SB RAS

Preprint submitted to Advances in Space Research April 15, 2017 1. Introduction The waves in solar magnetic structures play an important role in pro- cesses of the energy exchange. Moreover, the properties of the medium, i.e. the solar atmosphere, can be determined by studying the wave propagation. This affects such problems as the origin of the solar magnetic fields, coro- nal heating, flares, wave propagation in plasma with different magnetic field topology, and others. From the observation driven point of view the prob- lems above depend on our knowledge of the magnetic field distribution with height, plasma velocity, temperature and their variations. Because direct measurement of these parameters is a considerable challenge, in practice one has to use different tools to get a comprehensive picture of the atmosphere structure in active regions and processes therein. The seismological study of the active regions is one of such unique tools (Bogdan and Judge, 2006; De Moortel and Nakariakov, 2012). Different methods were developed to explore magnetic geometry of the sunspots and to estimate the magnetic field inclination angle in the transition region and in the corona (Jess et al., 2013; Yuan et al., 2014b; Kobanov et al., 2015). Coronal seismology pro- vides a capability to determine the magnetic field strength in coronal closed magnetic structures (Nakariakov and Ofman, 2001). Another opportunity is radio magnetography (Gelfreikh, 2004). The radio emission is naturally con- nected with magnetic field providing an instrument to study the 3D-structure of the sunspot atmosphere. Joint observations in radio and optical spectral ranges have a great potential (Kislyakov et al., 2006), that has not been implemented yet. One can trace the wave train propagation and utilise mag- netic field extrapolation to the corona to estimate the effective height of the radio emission, which can be used to qualify the formation heights of the lines in UV and optical spectral ranges. New facilities like the Siberian Solar Radio Telescope (SSRT, Lesovoi et al. 2012), the Chinese Spectral Radiohe- liograph (CSRH, Yan et al. 2013), and others will provide new possibilities for observing the Sun’s radio emission in the multifrequency mode. Sunspot oscillations were extensively studied in the past decades (see re- views by Lites(1992); Solanki(2003); Bogdan and Judge(2006); Jess et al. (2015)). Recent studies are based on multiwavelength observations and focus on determining the wave propagation speed (Felipe et al., 2010; Abramov- Maximov et al., 2011; Kiddie et al., 2012; Chandra et al., 2015), wave dy- namics (Sych et al., 2012; Sych and Nakariakov, 2014; Zhugzhda and Sych, 2014), and related phenomena like jets, penumbral filaments, umbral flashes

2 Fe I 6173 Å 1700 Å BII

60 2 40 arcsec 1 , kG II 20 0 B space,

0 0 20 40 60 0 20 40 60 0 20 40 60 space, arcsec

Figure 1: Sunspot NOAA11711. Left panel: SDO/HMI continuum image. Middle panel: the sunspot in the SDO/AIA 1700 A˚ band pass. Right panel: magnetic field normal projec- tion derived from the SDO/HMI vector data. The inner and outer penumbra boundaries are outlined by black and white solid lines. The dashed isoline marks the regions where the magnetic field inclines at 45 to the surface normal.

(Yurchyshyn et al., 2014, 2015; Esteban Pozuelo et al., 2015; Madsen et al., 2015; Louis et al., 2014; Maurya et al., 2013), light bridges (Yuan et al., 2014a; Yang et al., 2015) and also flares (Sych et al., 2014). Due to the circular symmetry, sunspots provide an opportunity to study the wave prop- agation processes in the presence of magnetic fields. In sunspot umbra, five- minute oscillations dominate at the photospheric level, and three-minute ones prevail in the (Kobanov, 1990; Kentischer and Mattig, 1995; Sigwarth and Mattig, 1997; Rouppe van der Voort et al., 2003; Kobanov et al., 2009; Reznikova and Shibasaki, 2012). Oscillations with longer periods (10–15 minutes) manifest themselves at the peripheral part of the sunspots. Other magnetic field regions, e.g. facula show very different behaviour of the spatial-frequency dependence (Kobanov and Pulyaev, 2007; Centeno et al., 2009). Detecting and studing the coronal counterparts of these waves and quasi-periodic pulsations are relevant for the problem of energy flux transfer to the upper atmosphere. We continue studing the space-frequency stratification of the oscillation processes in the sunspot atmosphere (Kobanov et al., 2015). We extend the analysis with new sunspot data, including those obtained in radio emission, and compare the results with magnetic field extrapolation.

3 2. Observational Data and Methods The paper is result of the investigation into the sunspot oscillations ob- served at different wavelengths representing several heights of the solar at- mosphere from the to the corona. We used the data from two observatories in this study: Solar Dynamics Observatory (SDO, Lemen et al. (2012); Scherrer et al.(2012); Woods et al.(2012)) and Nobeyama Radio- heliograph (NoRH, Nakajima et al. 1994). The data were selected to cover height scale from the photosphere to the corona. The sunspot had regular circular shape (Figure 1, left panel). The obser- vation was performed on 2013 April 6 00:00–04:20 UT and there was no flare activity at this period; a C1.7 flare occurred on 10:58 UT. We chose four spectral bands provided by the Atmospheric Imaging As- sembly (AIA) for the analysis: Fe ix 171 A˚ and Fe xii, xxiv 193 A˚ (coronal heights), He ii 304 A˚ (transition region) and 1700 A˚ (upper photosphere, Fig- ure 1, middle panel). The Helioseismic and Magnetic Imager (HMI) data were used to obtain the magnetic field at the photospheric level in the Fe i 6173 A˚ line, which is formed at the 100 – 150 km height (Fleck et al., 2011; Parnell and Beckers, 1969). The vector magnetic-field components were com- puted using the code of Very Fast Inversion of the Stokes Vector (Borrero et al., 2011). The SDO data sets were prepared using the aia_prep and hmi_prep SolarSoft routines. The sunspot was observed near the central meridian (W03S17), which allowed us to minimize the projection effect on the analysis of oscillations at different heights. We corrected the magnetic field angle to the solar normal within the planar approximation using equa- tion (Gary and Hagyard, 1990):

ϕ = cosγcosϕ0 + sinγsinϕ0cosθ (1) where γ is the angle between the line of sight and the solar normal; ϕ0 is the observed field inclination angle; θ is the azimuthal angle corrected for the line-of-sight deviation from the central-meridian plane (Figure 1, right panel). The radio data are the sequence of the 17 GHz NoRH images with the 20-second effective cadence and the 500 spatial resolution. The images were synthesised with the “Koshix” algorithm on the Solar Data Analysis System. To increase the signal-to-noise ratio, the number of integration frames for syn- thesis was set to 10. The images were cropped to include the sunspot area (400 × 40000). Then, the images were co-aligned using the cross-correlation

4 technique and smoothed over spatial dimensions. The maximum brightness temperature in the sunspot does not exceed 29000 K and the degree of polar- isation is about 25%. Thus, the polarised emission at 17 GHz in this image is most likely due to optically thin thermal bremsstrahlung. The line-of-sight magnetic field was estimated by the method proposed by Gelfreikh(2004). To study space-height properties of the sunspot oscillations we used the method described in Kobanov et al.(2015) that is suitable for circular sunspots. To calculate the cut-off frequency, we used the equation (Bel and Leroy, 1977; McIntosh and Jefferies, 2006; Botha et al., 2011):

g0γcosϕ(r) fc = (2) 4πvs

−2 where fc is the cut-off frequency; g0=274 m s is the gravitational constant; 5 vs is the speed of sound; γ = 3 is the adiabatic index; ϕ(r) is the dependence of inclination angle on the barycenter distance. Using Equation 2 and em- pirical ratio fc =0.81F(r) mHz−1 mHz for the 304 A˚ line (Yuan et al., 2014b) we estimate the magnetic-field inclination angle [ϕ](Kobanov et al.(2015)):

4πv F (r) ϕ = arccos s (3) g0γ The oscillations’ power spectrum was calculated using the Fast Fourier Transform (FFT). To remove trends from the data we subtracted the time series smoothed over a 25-minute time interval from the original series. The data set temporal resolution varies from 12 to 45 s for different instruments and bandpasses, which allows us to analyse frequencies up to 11 mHz — the Nyquist frequency for the HMI data; the Nyquist frequencies for the AIA data are 21 mHz (the 1700 A˚ band) and 42 mHz (the 304 A˚ and 171 A˚ bands), and that for the NoRH data is 25 mHz. To analyse the spatial distribution of the dominant frequencies, we obtain FFT power maps in the following way. FFT power spectra were calculated for every pixel (0.6 × 0.6 arcsec2) of the SDO/AIA/HMI intensity images. The calculated Fourier spectra were smoothed by convolution with a rectangular window 1 mHz wide. The frequency corresponding to the power spectrum maximum value was taken as the dominant frequency for the particular spatial domain. To analyse wave trains and to measure their propagation speeds the frequency filtration was performed by the sixth-order Morlet wavelet. We used the algorithm described by Torrence and Compo(1998) to derive the FFT power

5 Fe I 6173 Å 1700 Å

60

40

20 8

0 arcsec He II 304 Å Fe IX 171 Å , mHz space, 60 frequency 1 40

20

0 0 20 40 60 0 20 40 60 space, arcsec

Figure 2: Spatial distributions of dominant frequencies from the photosphere to the corona. The black solid lines mark the inner and outer penumbral boundaries. spectra, to wavelet-filter the data and estimate the statistical significance. The normalisation by 1/σ2 gives a measure of the power relative to the white noise level: 3σ2 correspond to the 95% confidence level, and 4.6σ2 — 99% confidence level (σ2 is the variance of a time series). The coronal magnetic field was calculated in the potential and nonlinear force-free (NLFF) approach, using SDO/HMI vector magnetograms as input data. To remove 180° ambiguity in the direction of filed component transver- sal to the line-of-sight we used the SFQ method by Rudenko and Anfinogen- tov(2014). The potential field was calculated using the method, described in Alissandrakis(1981) by applying FFT. The NLFF reconstruction was per- formed by using the optimization method, proposed by Wheatland et al. (2000). This method implementation by Rudenko and Myshyakov(2009) was used in the present study: we take into account a full set of the evolu- tionary equations and allow the field variations not only in the inner volume but also on the lateral and top boundaries of the computational domain.

6 8 He II 304 Å Fe I 6173 Å 2 6 1700 Å

BII 4 1 II B , kG 2 frequency, mHz frequency, 0 0 10 200 30

8 He II 304 Å Fe I 6173 Å 6 1700 Å fc 4

2 frequency, mHz frequency, 0 10 200 30 0 He II 304 Å 20 Fe I 6173 Å Bnp 40 Bp 60

magnetic  eld 80

inclination φ , degree 10 200 30 distance from barycentre, arcsec

Figure 3: Upper panel: dominant frequencies at three heights, and the magnetic field as a function of distance from the sunspot barycentre. Middle panel: dominant frequencies and the cut-off frequency derived from Equation 2. Bottom panel: magnetic field inclination angle derived from Equation 3 for the He ii 304 A˚ level, HMI Fe i 6173 A˚ data, potential (Bp) and nonlinear force-free (Bnp) magnetic field extrapolation at the 2200 km level.

7 3. Results Figure 2 shows the spatial distribution of dominant frequencies in the sunspot at different heights from the photosphere to the corona. The black solid lines mark the inner and outer penumbra boundaries. Five-minute os- cillations concentrate in an annular area, that expands beyond the umbra boundaries with increasing height. Low-frequency oscillations appear in the lower photosphere of the penumbra. Such a topology resembles the con- cept explaining running penumbral waves as upwardly propagating waves that form a visual pattern (Rouppe van der Voort et al., 2003; Bloomfield et al., 2007; Kobanov et al., 2009). Low-frequency oscillations occupy the larger area in the picture plane at higher coronal level visible in Fe ix 171 A:˚ the areas of dominant frequencies become elongated in the radial direction. Using the circular-shaped power distribution, one can plot frequency vs. dis- tance from the barycentre for different height levels observed with AIA and HMI. Figure 3 presents a dominant frequency [F (r)] averaged over the pixels located at distance r from the sunspot barycentre with a 0.600 step. The same averaging was used to obtain the longitudinal magnetic field [Bq] and the absolute value of the magnetic-field inclination (Figure 3). We estimate the cut-off frequency fc (Figure 3, middle panel) and the magnetic-field in- clination angle [ϕ](Figure 3, bottom panel) by Equations2 and3. Using potential Bp and nonlinear force-free Bnp magnetic field extrapolation data we produce [ϕ] vs. distance from barycentre plots for the 2200 km level. Both cases show a very similar dependence except for the outer penumbra (Fig- ure 3, bottom panel). In the Figure 3 middle panel one can see a penumbra region, in which the dominant frequency curve (304 A)˚ follows the cut-off fre- quency curve. Earlier, Kuridze et al.(2009) showed that pressure impulses engendered in the photosphere can excite oscillations at the cut-off frequency. Consequently, the oscillations that coincide with the resonant frequencies of the cavities under the magnetic canopy amplify and can penetrate into the upper layers of the solar atmosphere (Srivastava et al., 2008). High-frequency waves of the 6 – 7 mHz band concentrate at the sunspot central umbral part at all heights and form fragmented domains on the power maps (Figure 4). The power maps were produced by using entire time series. The NoRH at 17 GHz observation clearly show three-minute band oscillations in Stokes V polarisation channel (Figure 5). For the optically thin radiation the line-of-sight magnetic field can be estimated according to Gelfreikh(2004) and is about 730 G. Extrapolation of the photospheric magnetic field to the

8 iue4 nest F oe asaeae nte67mzbn.Tebaksldlines solid black The band. boundaries. mHz penumbral 6–7 outer the and in inner averaged the maps power mark FFT Intensity 4: Figure

space, arcsec 60 60 20 20 40 40 0 0 0 20 Fe He I II 6173 40 304 Å Å space, 60 arcsec 0 9 20 Fe 1700 IX 40 171 Å Å 60 max min

FFT power, arbitrary units NoRH, 17 Ghz, Stokes V He II 304 Å

60

40 arcsec

20 space,

0 0 20 40 60 0 20 40 60 12 units 2 8 σ , power

4 FFT 0 2 4 6 8 10 2 4 6 8 10 frequency, mHz

Figure 5: Left panel: FFT power spectrum of the NoRH 17 GHz Stokes V signal. Right panel: FFT power spectrum of the He ii 304 A˚ intensity. The signals were averaged over the area marked by the rectangle. The inner and outer penumbra boundaries are outlined by white solid lines.

4 1600 Å 3 He II 304 Å 2 17 GHz (Stokes V) 1 0 -1 arbitrary inits -2 -3 -4 0 20 40 60 80 100 120 time, min

Figure 6: Intensity variations revealing wave trains in the three-minute band in the chro- mospheric and transition region lines and the NoRH 17 GHz Stokes V.

10 power distribution 2.8-3.8 mHz 1-2 mHz intensity (non ltered)

60

40

20 space, arcsec

0 0 20 40 60 0 20 40 60 0 20 40 60 space, arcsec full eld of view 5 4

2 3 2

1 FFT power, σ power, FFT units 0 1 2 3 4 5 frequency, mHz

Figure 7: Fan-like structures in spatial localisations of low-frequency coronal oscillations (panels 1 and 2) and inverse sunspot image in the Fe ix 171 A˚ band (panel 3). Panel 4: FFT power spectrum calculated over the whole field-of-view. The inner and outer penumbra boundaries are outlined by black and white solid lines.

11 8 2 6 2 1

4 0

2 -1 FFT power, σ power, FFT units -2 0 2 4 6 8 0 20 40 60 80 100 120

frequency, mHz arbitrary units  ltered intensity, time, min

Figure 8: Oscillation behaviour in coronal loops above sunspot. Left panel shows the intensity oscillation power spectra in the loop points marked with crosses in Figure7. The results of frequency wavelet filtration are presented in the right panel. The thick lines show spectra and signals at the points located farther from the sunspot centre. upper atmosphere gives us the effective height of 2100–2200 km for the radio emission that corresponds to the transition region and the field strength of that value. Intensity variations in the narrow band of 3 minute for the 1600 and 304 A˚ bands show a wave train structure that is typical of sunspots. Similar structures are present in the NoRH 17 GHz polarisation signal (Figure 6). The measured time delay of three-minute propagating waves (Figure 6) from the level of 1000–1300 km (1600 A)˚ to a height of 17 GHz emission gives a value of about 65 seconds, and 5 seconds from the level of 2200 km (304 A)˚ to a height of 17 GHz emission. We can conclude that the calculated height of radio emission generation agrees with height estimations for other spectral lines (Avrett and Loeser, 2008; Zhang et al., 1998) and with the analysis of characteristics of propagating three-minute waves (Reznikova et al., 2012; Kobanov et al., 2013). At the coronal heights, power maps reveal elongated structures that out- line the coronal loops best at the 1–2 mHz filtration band (Figure 7). Sim- ilarly to the two sunspots analysed in Kobanov et al.(2015), the 1–2 mHz band oscillations can be traced along the loops to find the time delay and propagating speed. For this purpose we find two points along the loop hav- ing almost identical FFT spectra. These points are marked with crosses in Figure 7. Then using the amplitude vs. time plot (Figure 6), we estimate the apparent propagation speed that appears to be ∼45 km/s. The angle be- tween the line of sight and the considered coronal fan was estimated from the

12 magnetic field extrapolation and was found to be about 40°. Taking into ac- count this value we find the deprojected wave propagation speed to be about 70 km/s. This value is lower than the expected sound speed in the corona. However, it is consistent with other measurements of the slow MHD wave propagation speed in coronal loops, ranging from 20 km/s to 190 km/s (See Table 2 in De Moortel(2009)). It is interesting to note that low-frequency oscillations of 1–2 mHz band in sunspots can be connected with Evershed flow’s pulsations (Rimmele, 1995; Kobanov and Makarchik, 2004). The study of such a possible connection would require sunspots located near the solar disc limb. Other possible scenarios can be related to the stochastic motion of coronal loops or the non-damping transverse oscillations (Nistic`oet al., 2013; Anfinogentov et al., 2013).

4. Conclusions The 5–7 mHz band high frequency oscillations concentrate inside small- scale elements in umbra and at the umbra-penumbra boundary. These kinds of oscillations show a well-known wave-train behaviour that also reveals it- self in the NoRH Stokes V 17 GHz data. The wave trains observed in UV and radio coincide with a cross-correlation coefficient up to 0.75–0.92. The time delays for the 1600 A,˚ 304 A˚ and the NoRH signal agree with the previ- ous results, obtained without radio data analysis, and indicate that the radio emission effective height is within the 2100–2200 km range which corresponds to the transition region and the magnetic field B∼730 G. This value agrees with one measured in He i 10830 A˚ line B∼600–1500 G, (Solanki et al., 2006) and is much higher than the estimated magnetic field at the coronal levels B∼10 G (Nakariakov and Ofman, 2001; Zaqarashvili et al., 2013). The esti- mation of the magnetic fields at higher coronal levels would be possible with availability of new high cadence and frequency radio data from SSRT and CSRH instruments. The 1–2 mHz band low-frequency waves in NOAA 11711 reproduce the behaviour of NOAA 11479 and NOAA 11311 analysed by Kobanov et al. (2015): the power of these waves is concentrated in the annular zone around penumbra that expands with height. The estimated deprojected propagation speed of the wave train travelling along the single fan-loop is about 70 km/s. The magnetic field inclination angle [ϕ] in the sunspot was estimated in two independent ways: from the observations of the dominant oscillations frequency and by using the magnetic field extrapolation. [ϕ] derived from

13 HMI photospheric data is ∼35–40° for the umbra-penumbra boundary (1200 from the sunspot centre), and corresponds to the field extrapolation results at the 2200 km level (Figure 3). [ϕ] is obtained from indirect measurements for He ii 304 A˚ line is ∼40–45°. The inclination estimation results fit in with the general structure of a sunspot and provide grounds for new research.

Acknowledgements. We acknowledge the NASA/SDO and NoRH science teams for provid- ing the data. This work was partly done out on the Solar Data Analysis System operated by the Astronomy Data Center in cooperation with the Nobeyama Solar Radio Observatory of the National Astronomical Observatory of Japan. This study was supported by Projects No. 16.3.2, 16.3.3 of ISTP SB RAS, by the Russian Foundation for Basic Research under grants No. 12-02-33110 mol a ved, 15-32-20504 mol a ved, 15-02-03717-a, 15-02-01077-a, 15-02-01089-a, 13-02-00044-a, 15-02-03835-a. We are grateful to anonymous reviewers for their helpful remarks and suggestions. We acknowledge Y.M. Kaplunenko for his help in preparing the English version of the paper.

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